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31M13NW8897 63.3246 PACAUD 010
PROGRESS REPORT
ON
THE CATHARINE-PACAUD TOWNSHIPS PROPERTY
OF
WARREN EXPLORATIONS LIMITED
BOSTON CREEK AREA
DISTRICT OF TEMISKAMING
ONTARIO1C L-
j
By: J. A. Pollock, P.Eng.Dated at Haileybury, Ontario February 12, 1975.
SUMMARY OF WORK PROGRAM
CATHARINE-PACAUD TOWNSHIPS PROPERTYof
WARREN EXPLORATIONS LIMITEDBOSTON CREEK AREA
DISTRICT OF TEMISKAMING ONTARIO
(1) The property consists of two groups of patented and unpatented
claims totalling 1,272 acres.
(2) From September, 1974 until January, 1975 linecutting, geophysical
work, prospecting, trenching and diamond drilling were carried out.
(3) A VLF electromagnetic survey revealed four areas of minor
conductivity which should be confirmed with another type of
instrument.
(4) Trenching revealed scattered copper mineralization over a length
of 400 feet.\
(5) Drilling two short holes encountered only minor copper mineralization.
(6) The exploration program was aborted due to the arrival of winter.
(7) A further exploration program is recommended to further test
the main group of claims worked on, as well as to explore the
group of claims to the south to verify airborne anomalies.
(8) The recommended program should be considered in two phases:
Phase I - Geophysical work and mapping. Cost ... $11,500.00
Phase II - Depending on the results of Phase I,and supervision.
Cost ... $28.000.00
Total ... S39 1 500.00 '* l
POLLOCKr id "" " "
February 12, 1975. ' ~n A. Pollock, P.Eng.
- 2 -
INTRODUCTION;
In the early 1920's the Boston Creek Area was actively prospected
for gold and a limited production was obtained from two properties*
In 1926 copper was discovered along a zone extending south
easterly for 2-1/2 miles from the village of Boston Creek. Between
1927 and 1930 a limited production was obtained by underground development
of three properties.
Similar rocks extend in a semicircular belt along the periphery
of the granite through Catharine Township and contain a number of known
gold and copper showings.
During 1974 Jonpol Explorations Limited purchased two contiguous
patented lots for $6,000.00 cash and a 3 7, royalty based on net smelter
returns to a maximum of one million dollars, thereafter the royalty will
be reduced to 2% of net smelter returns t Jonpol Explorations Limited
vended the property to Warren Explorations Limited for a stock consideration.
In October 1974 the adjoining area was prospected as well as the
original Warren patented claims. The examination of the copper showing
reported on in 1929 by Victor James of Wright, Boydell James and Associates
led to the acquisition by optioning and staking all available adjoining
favourable ground.
A limited geophysical program was undertaken as well as" prospecting,
drilling and trenching. The arrival of winter brought an end to the operation
on January l, 1975. Work was confined to 952 contiguous acres around the
Old Mindoka Mines property.
- 3 -
The following reports, maps and drill logs have been referred
to and incorporated in this report:
Cunningham, L.J. - Mining Engineer - Report on Catharine-Pacaud
Townships Property of Warren Explorations Limited and
amendment July 3, 1974;
Cunningham, L.J. - Report on a VLF-EM survey on a limited grid in
Lot 11, Con.IV., Catharine Township, District of Temiskaming
for Warren Explorations Limited, February 10, 1975;
Cunningham, L.J. - Report ^n a VLF-EM survey on a limited grid over
parts of 2 patented lots, Catharine-Pacaud Townships, District
of Temiskaming for Warren Explorations Limited, February 10, 1975;
Pollock, J.A. - Professional Engineer - Letter to Shareholders of
Warren Explorations Limited, January 18, 1975;
Pollock, J.A. - Diamond Drill Records of Holes W-l and W-2 drilled
December, 1974;
James, Victor A. - Mining Engineer - Report on Mindoka Mines Limited,
July, 1929;
Grant J. A. - Geologist - Geological Map 2043 to accompany O.D.M.
Geological Report No.18, July, 1963.
LOCATION AND ACCESSIBILITY;
The property lies approximately 14 miles southeast of the
town of Kirkland Lake. The claims are 8 miles east of Highway 112.
- 4 -
Highway 564, an all-weather gravel road, extends easterly from Highway
112 through the village of Boston Creek and then turns southerly to
cross the centre of the property along the Pacaud-Catharine Township
line.
A high tension power line of the Ontario Hydro Electric
Commission and the Ontario Northman d Railway are located about 3/4
of a mile southwest of the property. The railroad is accessible by
an all-weather gravel road, the distance from the property being
three miles.
PROPERTY DESCRIPTION AND LOCATION;
The present Warren Explorations Limited holdings contain 952
contiguous acres and a separate group of claims containing 320 acres.
The description and status of their holdings may be described as follows:
Patented Lots held 10(^ by Warren Explorations Limited
Pacaud Township - S-l/2 lot l Con IV
Catharine Township - S-l/2 Lot 12 Con IV
Patented Lot owned by Gawley Estate Optioned to Warren Explorations Limited
Catharine Township - S-l/2 Lot II Con IV
Unpatented Claims held by Mr. Dave Bell and optioned to Warren Explorations Limited
L-380998 - SE 1/4, N 1/2 Lot II Con IV Catharine Township
L^-380999 - SW 1/4, N 1/2 Lot II Con IV Catharine Township
L-381000 - NW 1/4, N 1/2 Lot II Con IV Catharine Township
L-381001 - NE 1/4, N 1/2 Lot II Con IV Catharine Township
- 5 -
Unpatented Claims held by Warren Explorations Limited
L-406691, 92, 93, 94 being the N 1/2 Lot H Con III, Catharine Township.
L-406695 being the NW 1/4, S 1/2 Lot 10 Con IV, Catharine Township.
L-406696 being the SW 1/4, S 1/2 Lot 10 Con IV, Catharine Township.
L-406697 being the NW 1/4, N 1/2 Lot 10 Con III, Catharine Township.
L-400698 being the SW 1/4, N 1/2 Lot 10 Con III. Catharine Township.
TOTAL: 952 Acres
The company also holds a group of 8 contiguous mining claims
in the southwest corner of Catharine Township which may be described
as follows:
Unpatented claims held by John Duncan and optioned to Warren Explorations Limited
L-401751 - NE 1/4, N 1/2 Lot 11 Con 2 Catharine Township
. L-401752 - SE 1/4, N 1/2 Lot 11 Con 2 Catharine Township.
Unpatented claims owned by the Company
L-418698 - NW 1/4, N 1/2 Lot 11 Con 2 Catharine Township
L-418699 - SW 1/4, N 1/2 Lot 11 Con 2 Catharine Township
L-418700 - NW 1/4, S 1/2 Lot 11 Con 2 Catharine Township
L-418701 - SW 1/4, S 1/2 Lot 11 Con 2 Catharine Township
L-418702 - NE 1/4, S 1/2 Lot 11 Con 2 Catharine Township
L-418703 - SE 1/4, S 1/2 Lot 11 Con 2 Catharine Township
TOTAL: 320 acres
There was no work done on the above 320 acres during the 1974
exploration season.
- 6 -
GEOLOGY;
(1) General Geology.
(2) Geology of Property.
(3) Economic Geology of the area.
(4) Economic Geology of the property.
For the above, please refer to the incorporated reported by L. J. Cunningham,
June 25, 1974.
1974 EXPLORATION PROGRAM;
During the period between September, 1974 and January, 1975
an exploration program following the recommendations made by L. J.
Cunningham was conducted.
Picket lines were cut at 200-foot intervale over the known vein
areas and .V.L.F. surveys completed over the two grids. (Ref: enclosed
surveys by L. J. Cunningham.)
Several trenches were blasted into, on the Gawley option, and
the area around these was prospected. The mineralization in the trenches
did not respond to the V.L.F. instrument. The late season did not allow
us to map in detail these trenches but we expect to do this next spring.
An excellent description of the trenched area is given by Victor James,
Mining Engineer, in his Report on the Property of The Mindoka Mines
Limited, which is enclosed herewith.
Two short diamond drill holes were put down under what appeared
to be the best mineralization in the trenches. It was necessary to stop
drilling with inconclusive results due to the light drill equipment and
the cold weather. The two short holes revealed only scattered blebs of
chalcopyrite. (Ref: enclosed drill records logged by John A. Pollock, P.Eng.)
*- 7 -
A study was made of the results of the Questor Mark M.K.V.
input survey which was flown over Catharine Township in 1970. Four
conductors were indicated by this survey to the south of the Warren
property and eight mining claims were acquired to cover the interesting
areas. No conductors showed up on the Warren property itself.
The results of this survey are available at the Mining
Recording Office, Kirkland Lake, Ontario.
CONCLUSIONS AND RECOMMENDATIONS:
The fall program in 1974 of linecutting, geophysical work and
very limited trenching and drilling did not reveal any economic deposits
of copper ore. The work was confined to known occurrences and did not
cover a large part of the property.
The trenching did reveal scattered copper mineralization over
a length of four hundred feet north of the Gawley shaft.
The diamond drilling showed only scattered chalcopyrite under
the best mineralization but the possible plunge of the pipe could easily
have been missed. Two short holes are not a very good test of mineralization
which stretches for fbur hundred feet, but it was impractical to continue
in the winter with the Winki Drill.
The geophysical work did reveal some conductors on both grids,
which although they do not appear strong should probably be tested with
more sophisticated instruments.
The group of 8 mining claims to the south which were staked to cover
weak airborne anomalies was not worked on at all due to the lack of time and
men on the project.
-f 8 -
It is recommended that:
Phase I; (1) Detailed magnetometer and electromagnetic surveys
be conducted over the present grids to verify
anomalies outlined by the V.L.F. survey.
Cost ... $ 6,000.00
(2) Detailed mapping be done on the grid areas
to tie in mineralization with geology.
Cost ... $ 1,500.00
(3) Anomalies on the southern group of claims
be verified by V.L.F. and further checked
with a more sophisticated instrument if
necessary. Cost ... $ 4,000.00
Phase II: Diamond drilling if warranted be completed to:
(1) finish testing the known mineralization
(2) test anomalous zones.
Cost 2,000' @ $12.00/ft. Cost ^24,000,00
Supervision 4.000.00
Total:
CERTIFICATE
I, John A. Pollock of 651 Latchford Street, Haileybury,
Ontario, do hereby certify that:
1.
2.
3.
4.
5.
6.
7.
I am a practicing Professional Engineer with offices at Suite 600, 85 Richmond Street West, Toronto, and Haileybury, Ontario.
l am a registered Professional Engineer of the Province of Ontario.
I have been working in the mining exploration business intermittently for 25 years and hold a 1950 Ontario Prospector's Licence.
I am an employee of Pioneer Consultants Limited and have been working as an engineer for them for over five years.
This report was compiled from information received from various consultants as well as first-hand knowledge gained by supervising the exploration program in 1974.
I was on this property many times between September, 1974 and January, 1975.
I am the President and major shareholder of Warren Explorations Limited. The control of Warren Explorations Limited is held by Jonpol Explorations Limited which is a private company controlled by myself.
Haileybury, Ontario,
February 12, 1975.
John A. Pollock, P.Eng.
31M13NW0097 63.3246 PACAUD
A VJ-iJ. —^fa^jt iM/wAt VAJ.L ON A LIMITED GRID
OVER PARTS OF 2 PATENTED LOTS CATHERINE-PACAUD TOWNSHIPS
BOSTON CREEK AREADISTRICT OF TEMISKAMING
ONTARIO
020
LOCATION 6 ACCESSIBILITY
The property consists of 2 contiguous patented lots, one in Pacaud
Township, the other in Catherine Township.
They are unnumbered but are described as follows?
Pacaud Township S^ Lot l Con. IV 160 acres
Catherine Township S^ Lot 12 Con. IV 152 acres
The property lies approximately 14 miles southeast of the Town of
Kirkland Lake. The claims are B miles east of Highway 112. Highway 564, an all-
weather gravel road, extends easterly from Highway 112 through the village of
Boston Creek and then turns southerly to cross the centre of the property along
the Pacaud-Catherine Townships line.
GEOLOGY OF THE PROPERTY
The eastern margin of the Round Lake pluton underlies parts of Lot 12
along the western edge of the property. The Keewatin rocks occur as a steep
anticlinal belt around the granite. Grant (O.D.M. G.R. 18) has subdivided these
rocks into three stratigraphic formations, from west to east and from oldest to
youngest as follows:
A. Interbedded tuff and tuffaceous sedimentary rocks; with minor iron formation
This division lies next to the Round Lake pluton and is traversed by numerous
small dikes and sills. The total thickness is unknown, but is about 1,300 feet here.
B. Dioritic, dacitic, and andesitic lavas. Pillowed lavas are common in this division, which has a thickness of about 10,000 feet.
C. Porphyritic and aphanitic, intermediate to acid volcanic rocks, largely
pyroclastic, and agglomerate. The thickness of this division is also about
10,000 feet.
ECONOMIC GEOLOGY
Two miles to the northwest of the Warren ground copper shoots have
been mined as replacement bodies in iron formation at the contact with acid tuff,
The mineralized zones are pipe-like and of high grade (5 to 10#
copper per ton) with maximum dimensions of 50 feet in length by 5 feet in width.
Warren, Boston Creek - 2 ~Feb. 1975
tThey appear to be localized at cross faults which cut the iron formation.
The ore consists of chalcopyrite with varying amounts of bornite,
chalcocite, pyrite and pyrrhotite. Mineralization grades rapidly from massive
chalcopyrite to barren pyrite and pyrrhotite.
Within 200 feet of the Pacaud-Catherine Township line in the north
west quarter of Lot 12, Con. IV Catherine Township, the caved collar of a small
shaft can be seen with a small rock dump. Caved and flooded trenches indicate the
presence of two veins which are described by Victor A. James, Mining Engineer, in a report dated 12th July, 1929 as follows:
"The westerly vein system occurs practically on the Pacaud-Catherine
Township line, very close to the granite contact. The contact itself lies in low
ground, but has been established by diamond drilling. Granitic dykes (or small
sills) also occur along the bedding planes of the tuffs near the veins.
The veins consist of stringers of fairly massive chalcopyrite,
together with about two feet of banded pyrite and chalcopyrite mineralization in
silicified tuffs. The veins follow the bedding of the tuffs and dip about 82
degrees east. Two of the main stringers are 45 feet apart. A vertical 2-compart-
ment shaft 100 feet deep was sunk on the easterly one, and 55 feet of crosscutting was done at the 100-ft. level."
FIELD PROCEDURE
A grid totalling 2 miles (8 lines 9 1,300 feet each) was centered over
the shaft which is located on line 0 + 00 approximately 250' west of the township
line in Pacaud Township. Readings were taken every 100 feet along the lines which
run approximately east-west. 110 readings were taken using the transmitter
station at Cutler, Maine.
An appendix is attached describing the VLF-JEM procedure.
INTERPRETATION OF RESULTS
The roads separate the areas of outcrop from the overburden-covered
areas. East of the main north-south road and north of the east-west road which
crosses L 10 4- 00 S, the ground is high with much outcrop. In this area is
located the shaft and a number of pits; however, no conductors were encountered.
The balance of the property is covered by clay overburden cut by deep,
steep sided ravines. All of the conductors were located in a north-south
direction lying 100 to 300 feet west of and roughly parallel to the main road.
Overburden in this area is estimated at a minimum of 25 feet. The conductors
appear conformable with the general geology. It has been the writer's
Warren, Boston Creek- 3 -
Feb. 197i
experience that topographical conditions as exist here commonly produce a conductc
at or near the interface between the clay overburden and the rock outcrop. This
is not the case here - the conductors lie a minimum of 300 feet west of the
overburden-outcrop interface.
Because the conductive zone parallels the known mineralization it is
recommended that it be tested by more sophisticated geophysical techniques.
Dated atKirkland Lake, Ontario10th February, 1975
L. J." Cunningham, B.Sc., P. Eng., Mining Engineer
' * , * ' 1 ; * * *
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hadars •equij-iwnt oiraply utiilxoo a radio r^coiwr cowtrin^ the band of V 'LS* tivnnriittor aUitiona (scattered ov^r thia continent and
parts of tho world. 'ttwaa tr-ittccdtter tesoa ara aafx/cially construct ed tawora which tr.ink*it on the VLF froqtnmcy (vory low frequency) tvxprfcosly Tor cojaunicut.'.on with tiuLr^u-Anuu x/fiich they do effective!,/ through depths of salt water. Thsroi'om It ia underfit ndable that penetration into i\*ck lo substantial bJiould the** be rio cc-fKixicti^o ovorlaii-dlon acting ao an inhibitor.
st&tiona transmit in t!io 17 Tea. to 26 f'cu. run- re. A station Is choaciii DO t?u;t Uia elttctroria, .^ictic lines of i'orctt of tl;o horiac*iuj,lly cc-nctsitric i'ioid are i^rjxmilicular to Uio istriko of the or corv.Juotrore which tu-o boii^ oou^ht in the rc&ion of JUttcr^at. Iho VU' jj^itiona available jikiictr it u slwjjlo natUu" to aoloct U:o oppropri;.ito
fitud ill/'oetion rti^iiirud which vf;ia the Cutler, f*kino sUition ij.i tho ce&e. 'ilso troncsuittfrr stiitiois way olwwt bc conslcUirod as loeateci r.t i tliorciors; the primry fluid io uiiforo ft.nd parallel iri a givers area.
Coupling due to a at conclary induct flold is raeaour^d by a tiltis accoui.vLi^hoci by tvirning the rwcoiver around a vertical axifj
to a position of Kiniriu;^ oi;?tial ond then tiltiiif, around a hori;;wstal axis to a pooitifin of no ui^i-al or "null". Tula wvlo is wtsiimir^d in tio&roea txtjtil UK*
oi dip ia luxttd. Thw receiver la trarked JK) thut wtien t,llt*Mt fmfistn^v-Ttt rsoir.t tcwani tho axis oi' the conductor, /.t) thtj
conductive axis io Hci\)cDod over" the arrow r^iiittt v^rticalXv liown wid tho dip iiriglo is ccro. Vho Uc,-jrye of tilt or amplitude io gonoi'.-iily a r -^svrfc of tho intensity of iho conductor. The './idtt; bot^.1' ori tho jxsftka of the uaplitucis ia generally mi isulle.;tlori of tho depth of tho conductor. The mrrowt'r upre/td of
pucUc in'iicatin/} a conductor noaror curface.
JUidom InoVrMKient raist bo used \*ith a *jrofit doal of (ll9cr*;tion and the froo,uc-*icirso ua*xl eiftjdlar3.y ax.teniiaito Uu'ifd itiotailic conductora
otrwig surficial ionic couuuotore. 'iije roaaltant conduetivo aonoa raay to aulphidoi}f faults, v?et alioara or surficial conductive clay.
This is a rugged, simple to operate, ONE MAN EM unit. It can be used without line cutting and is thus ideally suited for ground location of airborne conductors and the checking out of mineral showings. This instrument utilizes higher than normal EM frequencies and is capable of detecting disseminated sulphide deposits and small sulphide bodies,, It accurately isolates banded conductors and operates through areas of high hydro noise. The method is capable of deep penetration but due to the high frequency used its penetration is limited in areas of clay and conductive overburden
The dip angle measurement detects a conductor from a considerable distance and is used primarily for locating conductors. The field strength measurement is used to define the shape and attitude of the conductor. *
31M13NW0097 63.3846 PACAUD 030
t
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REPORTON
A VLP-EM SURVEYON A LIMITED (HODIN LOT II CON. XVCATHERINE TOWNSHIP
DISTRICT O? lEMISKAMINQONTARIO
LOCATION t ACCESSIBILITY
The area lies in the KB 1/4 of the 8 1/2 of Lot H Con. IV, Catherine Township.
The property lies approximately 14 miles southeast of the fown of Kirkland Lake and 8 miles east of Highway 112* Highway 564, an all-weathor gravel) road, extends easterly fron Highway 112 through the village of Boston Creek and then turns southerly to parallel ths Buoaud-Catherino Townships line* Near the centre of the S 1/2 of Lot 12 Con* XV a tractor road extends northeasterly to the NE 1/4 S I/2 Lot 11 Con. XV, a distance of approximately one Rile.
GENERAL GKOLOQY
Keewatin volcanic rooks underlie most of tho aroaj immediately to the west is the Round Lake granitic pluton, with its Margin convex to tho oast* In general conformity with this margin are i (a) banded tuff, (b) basic to inter mediate lavas and intrusions, (o) Intermediate to acid fragmental rooks, and (d) coarse-grained volcanic rooks.
The Keewatin rooks were intruded first by ultrabasic to intermediate dikes snd sills, and then by numerous, small acid to intermediate, and lampro- pyriokdikes - probably r associated with the emplacement of the Round lake pluton.
*"t " : ,;; , '
QEOLQQY OF THS GRID AREA
The band of basic to intermediate lavas with intrusive* is approximately two miles wide* The flows strike northerly. The grid is oontfced on a shaft which is located on a felsic tuff horitton intercalated within the volcanic flows.
PltOCBDURE
A grid totalling 14,000 feet was out over the shaft area. From a base line (approximately north-south), 14 lines, 1000 foot in length, were out at 200 foot centres. Using Cutler, Maine as a transmitter station, a survey was conducted over the grid. Approximately 140 readings were taken*
An appendix is attached describing the VLF-SH procedure.
l
t
Karren, Boston Creek
INTERPRETATION OF RESULTS
Wb. 1975
The terrain is one of considerable outerop separated by Mall areas of overburden. Two streams traverse the ground*
Two conductors are considered to be worthy of further investigation by nore sophisticated geophysical teohniques* They fret(1) The conductor which crosses 1*12861143 at approximately l -f 50 west of base line and(2) the conductor which crosses X* 14 S and L 16 3 approximately 100 feet oast of base line.
The remaining four conductors are strongly suspected of being due to conductive overburden.
Signed,
Dated atKirkland Lake, Ontario10th February, 1975
Engineer
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kadota oquirwmt aiwply utilises a radio receiver covering the frequency band of VL;' ir nadtior stations eeiituirod ovtr this continent wnd other parts of tb*j world* 'iticso tr*mordtu?r buaoci arc oapociolly constructed towers which tr.yVa-.iit at the VIJ.' frocjwmcy (vary low frequency) exprfcosly ior (xx:*iuriicat.v.on ViJiti; ouUyjr.urieu wriich tJwy do effectively through depths ol
vator, 'flwrei'ore it ia underat nda:.lo th&t penetration into rock ioLe no conductive ovor burden acting ao taj inhibitor.
"ticac trrsnasittcr atitions trana-sit In tho 17 Kca. to 26 ?rca. run --e A station is cJtosRi! RO t!iat - .-!.a isiectra^. rnofcic linuo of fore** of tlie horiacii tally cwcoi-itrie i'ioid are ixurixmdioular to i ho etriko oT the Tcr^itic-n or cwi'.luotore wJiicJ*. ar*s "woitvj fcoufht -In tiie re^oti of interest, 'the numerous VU' atistiorjo available mko it ci siaplo natter to select U:o ftppi-oprifito priJ.!K',ry I'if.-idi d.L- ic:ction rt^iiir-wd wJi.icJi v^ao the Cutler, .-feiijici ettition in tho
case. 7h0 trcins&ittor atation r.say uljsoat bc c*^isi(J^rod as loeatcd at thwel'ore l he priraitry field io uniform fmd parallel in a given area.
Coupling due to a ot condary iridxiced flold is neaaurwd by a tilt Tills is accoi^xLish'Jt! by tiutiing the rwcoiv^i* around a vcu^tic-ii axis
to a r*o3iticn of ninii::ui': sij^rial ^md thun tiitliy, around tt horizontal a^cis to s position of no uiyyri-al or "null". Thio fiiv.*lo is r.easuryd in do,^rowo 'JJd tlie direction oi tlip io noted. Thw rcceivor ia catted so thut wtion tilt*M.t on arrow on LJ;o inotrj-^vr.t ix/ir.t towaixi Uio ajtia OA tho cc^idu^tor* , .o the conductive oxio io "crocood ovs^r" the torow iwitits vertically viwfln euid tho dip iini^Lo is ccro. Vho dc;;rue ol tilt or amplitude io gtsnoivuly a r .w*suj^ of tho intensity of tho ctjnductor. Tbo wi-ith betw- ori the pu^ks oi the amplitude ia gesaerfj.ly mi ln;ilc.vtiori of Urn depth of the conductor. The narrowor spre^id of tho ]xx*Jc Inviicfiitin/j a conductor nearer eurl'tice.
Iladcra instrument nust bo us^d vith ft ^jrcat deal of (d9cr*;tion and exjx^rienco; the fre*.:uenciGo uaod eimilarly attitfiuato Luri*id not&lllo conductoi*0 atid otrung ouj-ficiol ionic coiciuotore*. The resultant conductive ?x)ru*a raoy to graphite, oululiicioi?, Iiiults, v;et trtioara or surficial conductive clny*
This is a rugged, simple to operate, ONE MAN EM unit. It can be used without line cutting and is thus ideally suited for ground location of airborne conductors and the checking out of mineral showings. This instrument utilizes higher than normal KM frequencies and is capable of detecting disseminated sulphide deposits and small sulphide bodies,, It accurately isolates banded conductors and operates through areas of high hydro noise. The method is capable of deep penetration but due to the high frequency used its penetration is limited in areas of clay and conductive overburden,,
The dip angle measurement detects a conductor from a considerable distance and is used primarily for locating conductors. The field strength measurement is used to define the shape and attitude of the conductor,
WAKRfH emo* 040
FIELD OFFICE 8U1TE 4O ,P.O. BOX 38, HAILEYBURY, ONT. 36O BAY ST.. TORONTO. ONT.
PHONE 705-672-3311 PHONE 416-363-7381
WRIGHT, BOYDELL, JAMES & ASSOCIATES
REPORT
on property of
MINDOKA MINES LIMITED
Boston Creek Area,
Ontario.
SUMMARY;
Property of 640 acres, five miles by road south-east
of Boston Creek Station, three-quarters of a mile east of
Mindoka station on the T. S N. 0. Railway, to which road
is being completed by Ontario Government. Power line one-
half mile to west. Motor road crosses the property.
Two known vein systems, about three-quarters of a
mile apart, both striking west of north. The west vein
system is probably a southerly continuation of the Amity
break. The limited work done so far, including a shaft
100 feet deep, 55 feet of crosscutting, and 1100 feet of
diamond drilling discloses narrow widths of high grade
chalcopyrite and some disseminated low grade ore.
The east vein is newly discovered and appears to hold
such larger possibilities. It is in fact one of the best
surface copper showings in the whole district. The break
is strong and structurally well-defined. It has already
been traced for 1500 feet and it has every appearance of
continuing much further. The property covers the strike
for over one mile.
- 2 -
l! fl;
ll
channel eonploe token 10 and 14 faot bolov ourfaoo
in an Inollno ohnft guv a an average of 2*2;# copper over 4.5
.foot in width. Copper appearo coning in (nore strongly vi th
depth in thin shaft, aa tho surface eh owed no rely stringers
of copper oarbonatoa lying in tho broak. i
About 6DO foot north of this shaft, n discovery of
hi eh grade oro in thin voin was nade At tho tino of riuit,
undo r an apt urn o J. troo root* L c. re o e-nsulftr fragnonts ad
hering to tho troo root ohowod high crado o hale o pyrite oro
and on otripping, oro of the s aa e character was found in
pi GO o ovor ft width of fivo foot* — T*t6
this ohowing gavo 20*20^ copper over 6*0 foot and--'~
.. toaothor wi th trnooe of
gold* Stripping lo continuing on thie inportnnt discovery,
and chalcopyrite hao been found in tho vein for ndiotance- '-\- ' ' ." ' ' '."- '
of oeyorjil hundred foot* ?ho oro is of the replnoenont
typo* trith vory little Toin quarts*
Thio voln occurs as a troll-dofinod o true tar&l break in
Keewatin rocko, no ro or lose paralleling the contact of the
largo grnnito batholith to tho woot f a oot of conditione
which nay bo r^c/xrdod no vory favourable for otrongth end
continuity of ore in depth*
S'ho active dovolopcont of the o rv o t voin on thi o prop
erty, particvxlarly i ho area noar tho now discovery* is ro* oonnendol* : , ' :- .' : . - ; ;. :'. : .. -'. ; '- •"'-• i '" :-.' ;: '" ; . ; :','-.' : -
*#
P.J
*31!'
n:'
P HO ?V RT Y f
: ' ' ' ' ' - " , ' , ' r - -1 ' '
property conprleoa 640 aoroo in the surveyed totrn- ohips of Cftthorlne And Paoaud, Larder Lake Mining Pivloion,
Toniokanins District, Ontario* It includes tho whole of Lot
11 nnd tho south half of Lot 12, Cathorino toonshlp, and the
south half of Lot l , Pacaud township. -
Sono of thlo eroand is held, ae faro land e, carrying
both ninoral and earfftoe righto* Other portions are e take!
aa raining olalrne* Mo eoaroh of tho titloo waa nade*. ^ ' ' . - . . ' - ' 1
LOO A 'i
property lioa cloao in and lo onoily roaohod* Tho
orunpo nro oito&toi fivo nlloa oouth—eaat of Eooton Crook
station T)y road* night-of— tray la already oat for road to
Hind oka station on tho ?. ft W. O* Hailcay, a dietonco of
about l i: lailoo. Tho Ontario ,;ovornnont hne undertafcon to
conploto this road thio ounwor* tfho diroot dictanoo froa
tho proporty to tho railway le loss than ono-half nilo*
transnin.ionUino of tho Korthorn Ontario light
and Power Company pao808 a Bhort di O tanoo weot of tho; Prop.
orty.iuid i. vithlh onoailo of; alaoo t ony part of tho grptxp.
It io aloo po 03 lbl^ that* otoppod-dowi Toltano oould
obtained from .omo of tho noarby de Volo'p,ed :'; pro partio.."
A ' f^ ^
,p*',L 'it!-'.",-
'A sot of now camp building ha. bocn orectod/Uoo-
prioinc offloo, oookory nnd bunkhouno mifflolont for a
(Continued)
o row of 20 non. Several email crooks oro go tho claims and
domootio water la obtained frora veils* Tho country le
nootly burned over but thoro is sufficient standing dry
tinber for diamond drilling nnd domestic purposes* /Fuel
la not a problem horo on account of ready transportation*. ' , ' , .1 . ' : ' ' ' '" ' . ; : '~\ ."' , . " 'i :; ' L; ' ' , : ' "- ". .''"J • ••'. -'" ' i' ". ,. ' ' " ,
ns Y P ?.o P "R " '''''A nanber of othor coppor properties are boihn dovelopod
nearby. Chief amongst those aro tho OcoIan-TrethoBoy,
Patterson Copper andJAnity Copper, which lio to tho north of
the I'ihdofcft" fjroap in . tho order n&nod* ffhe voot veins on
the liindokn probably represent 'the southern extension o f
tho vein oy o 1 45i on tho above properties, on which pro perti ea' * '-' : ' "' " V ' - - S, ' ' . '.'' . .'.' ' , ' . ' ' r ' - , " " -' ' " ' . ' ,
ondorfrround work io at prooent procooding. A nxunbor of'.•••- ,'.':' - '' '-' '- ' ~ ' " ' ( ' ,V'y.;'".:':'- ; f y ' l'\,' V 'W:.V.' ' : ' :"' ' ' -" ; '"',
partly dovolopoi col* projw*rtioo ftloo lie to iho east and
' north or tho mndokn* , l -, . '-' ''' : ;V •:^:^^;i^-^A^;';";;'^^vK, :;l ; --:i.;-;iv.^ ; -.- ' . -' :v . . ' . ' . Si' ^ '•'.•,;:- - j. . ^^M/.r'^^''' 1 '''^.:^ '"i"; W'; '7" : "^vi"V : ,' :
G"OLOflYl
She ecology of the district and of the property is
relatively oitnplo* Tho Xeovmtin volcanics on the oast have, -'. ' ' - ' . ' - '-- : ' :'^.\. t: ^;f:^;I:ii^•:^^'^V^^^^-V••^ ; •'••
been intruded by a h use granite batholith which extends for: tsnny nileo to tho west and south* ?he intrusive contact
follows an arc having n-^onornl northwesterly trend* On '
tho ^Indokzv pro po r t/j, th e contact strikes f.bout 2S]de(?roo0
*eut of north, -Ahilo;farther to tho north r.oar Boston Creek
station it striJcoo nbout M650 weat. floar: :;thfli contnc* with'|.k
the volcnnico the fjrAnito tondo to naaumo a distinotly^ - t;;-
cuoinelo bcnilod utructuro. Lyinc next to tho uranite con*fix
tact io a band up to half a nllo t'ido of b o tide d tuffs and O
. 5 .
l c o n tlvolcanic fra^nontal rooks* Thin le ouooooiod to tho oant
by pillow Invan with nro&o of old diabase* narrow eranitio and
foloitJ.o dykoo occasionally occur cutting tho JToowatln rookfu
Tho ochlotooo Dtrixctura of tho Koowatin fratfraontal rooks and
tuffo conforno to thq gonoral dlrootion of tho granite contaoto
Aa noted lator,, thoro nro n imrabor of treriovoroo faults, ftl ong
t?hich tliero hao boon a oli{jht oovoncnt*
Moar tho northonct corner of tho property two apparently
asparuto tntruoionn of oonoidorablo else occur. Tho
Intraoion le A RIROB of cabbro^ crowded t-ith mgnotito
To tho woat of thlo thoro lo a largo dyfco^ 75 foot or nore
of nlcfv Innprophyro. Thooo two intraolono nro oopftratol by t*.
drnw or rolloy otrlktn^ poat of north*
(TAffi •W-'-.-'-v-.'** Wl
principal volno, or vein eye tons, oro knorn to
cxlot on tho proporty. She weotorly ,vcln syotcn occnro
practically on tho Pacaud-Cnthorino i'ownohip lino, very
clooo to th-j nrnnlto contact* Tho contact Itsolf lloo
In low croond, but har boon ootabllnhot! by dlcnond drill
!nc* Ornnltlo dykon { or onn.ll oille) also occur
tho boidJn,'j planoo of tho taffo near the volns.
5?ho voino consist of etrln^oro of fatrly
chalcopyrito, to;;othor vith txbout tvto foot of banded
pyrito juid cJmloopyrlto tilnoi-allftation in sillctfied
tuffs. 1'ho voins follow tho bncldinj of the tuffe nnd dip
aV.out b 2 rto^rnoo nay t* Two of tho nniri otrln -ore nro
foot ftpr*rt. A vortiorvl 2-oowpa rtr,c*nt shaft 100 foot
'.k on t!u o a j: t i? r J. y ono e r*.nd DD foot of
•rg
: Mf- 6 -
(Continod)
done at tiio 100-ft lovol. Vhoao workings nro now under
uator and tho Information below, obtained fron the nupor-
Intendont in charge, lo given RB ft rant tor of rooord.
Two drift roands on tho vein fron the vest oroon oat
shotjod 4?j copper over a cridth of 4 foot and 5^ copper over
4 foot, ' l
Foar dlsnond drill holes wore aloo pat dot?n. Throe of
thooo diocloeod oondltiono r&n^lng; froa nlnoralizntion to
oro. Tho boot holo showed 21 Inchon of core, roprooonting
10^ pluo inches true width, of rmaotvo ch&lcopyrito fxsnay-
2lcJ coppor. A 70-dogroe hole out 6 foot of vein natter~-.—— . -: -~~~ .
is 2.6)* copper*
In nonoralp it ntxy bo oald that this depth exploration
slightly bottoroii tho condition nppoarins on oarfftco, bat
the dlnonoionn ootabllohod to (Into nro rather too ecinJLl to
const!tato an ooononic deposit*
Ti'.ST V'.'IKi"--"
ffhio lo a parallel votn occurrlnc throe-quarters of R
nilo onot of tho i?oot voin end tho cane dietanoo onot of
ihe flranlto contact. Vhig lo a aaoh otrpn^er broak nnd
on.ro to hold wu oh Inr^or poonl bllltioo than tho voat voin*
Tho nroutrrr diotanco fron tho granite Is conoidorotl to
ijo an advr*,nt.-\no, rnthor thnn othornloo. Ihe ffonoral trend
of thlo vein lo north 20 degrees t/oot (nacnotlo) tind ite
ftvora^ro dip 7.0 do^roos onnt. A picket lino ran i n tho above
diroottor. wnn found to follow the roln fairly closely. The
vein' hno bo.-in traoed for 1500 foot on tho otrlko, and thero
lo no doubt obout l to furthor contlnutvnco oopeclnl Xy to
7
" o nt l nuod J
voin in plucoo followo a sheared or f united
contact botwocr. t\n o ld aie-bnne on tho voet nnd pillow Ifttrn
on tho or-.nt,, and It lo rmrJcoJ. by tho proatucoof a no. x- r or
dyko or rib of n, dontso greenish felsitic rock*
2? h o oro in tho voln lo of tho roplnoenent typo, tvoc-
orapnnlod by vory little c-ti\RrtP.a Chalcopyrite and, pyrJ.to
ropleco tho country rook B ooaetinos In frr.cturos And .fine
diosoninfttlono adjaoont to fine qanrtz otrlncorso sor.io*-
timoo oulphldoa rcplr.co It nltaost conplotcly in vhlch
caoo hi,-'h*.grr.do oro is tho rooa.lt*
' Xt io ftloo notable th&t n pinfc nranltic dyfce eovorol
foot wide outcrops within thirty foot to the vent of thia
rein In oovoral placoo*
A oorloa of trnnovorao faults^ otrlklnn raoro or JOBS
oaot and woo t, cat tho voln In ntxny placoo and diDplnco It.
f rota o- fow inohoo to R fow footo 'i'ho dl.splacenont in n early
alwayo to tho oust on tho north eldo of tho fi\Ult* Tho fault
flocuroo nro oonotinoo flllol with a fow Inchoc of qunrtsi
and tho voin nor\r them lo of ton onrlchod vi th quar t c and
nloo oul nhldo' nlnornllzatlon* Thlo action nppoare
Of tho diotrict* It lo notod ixloo on tho coot voln
on tho Ant t y Coppor lo tho nortl.vtoot, eh oro the "quarts
fftultn" dlsplftoo tho vein In the cfttae mariner ftnd oauoo ore
enrichment o In It* Tho qunrts t\p?oars lo onfxnftto i'ron tho
Crixnlto, vhich lo probnbly also tha coaroo of tho ooppor*
An incline ohaft lo bcinn sunk on tho oaat voin at
about tho centre of tho couth-OMitoriy ICO acres* At this
point tho ourfaoe thotto chiefly iron pyrite in tho voin,
with otrlji/roro tiiio^inR cooper curbonatoo nnd a littlo
l
chalcopyrtto. fho north t/nll of tho ohuffc choco chalco—
pyrl to coning In o4ulto ntron.;ly a o far R.O tho present bottom
of tho nhnft0 nt 15 foot. TTTO average or-7,plos acrono this
nail nt 10 foot r*nd 14 foot la dapth respectively shosrod
Io96;? coppor ovor 5 foot rind 2*6/5 coppor ovor 4 foot. She
appofcranco of tho oro lo bottor than thla and farther
check onnpllng till bo aono* She south wall of tho ehnft
ahotra IOSD chalcopyrlto bat lo hs.-vviljr shcnrod and shows
r. blr.olcinh jnlnornl rocenblins K^aphlto* Tho dyko or rib of
fnlslto npponro en tho hnnginn vrall*
Pron horfl tha rein is traced At froqaont intervale for
GOO foot to tho pouth c,nd 900 foot to the north. In man.?
plftcoj) it n.^poarc at tho ourfaco noroly aa a runty ^oosmn
eovorul foot ir. width, ohor/ing very liltlo r-alphide until
froohly blaotcd into* Cooper ninorclisation a;ipoc.rs rtron/jor
toward tho north. Tho bost indi vidu.nl oho&iiif; Wfto found
at tho tino of visit* Trr-cnonto of oro in nn uptxirnod
troo root woro found to bo ovorlyinc hi^h-ffrade ore in
oita* fitrippinj? disoloocd a width of nore than fire feet
of nearly nixon i vo oulphidoa, chiefly chalcopyrite. Channel
fjnnplo 'lo. 1001 noilnd r-crooo C. O foot hero ticrnyod 20.20^
copper, and n traoo of /:old. A fov foot tc the south,
nJm.nn*il o-;iplo Ho. 1502 Rcros^ ''...6 font r.fxvo c,lC;,^ copper Rttd
QQ*CO in paid, /."car tho t-nut:. end of Ihia ctrifiping sono
^rxlona vr.3 noted in the doooraposnd vain cu&ttor, a picked
cpccinon of vhich mn 12.00^ in load r.nd 50.0 os. eilvor,
also a traoo of .,old^ n rceult w hi o h lo ourpriein^ and, to
ony tho l o. tit, intoroBtin^. Snnploo 1901 nnd 1S02 vero not
(Continued)
a f-\"t'-: 't
S!
assayed for oliver, "but thin will now bo dona* in view o f
ft'oovo reuulta. '
Tho above eho*-ins is atout GbO foot north of tho in-
cXino ehaft. Strlpplnc wno proceeding north of thin again,
In tho courao of trhloh cood showings of chalcopyrite had bem
partly oxpooed in r* nunbnr of placoso Tho felsite dyko
follova.tho voin poraistontly rhorovor fiaao has boon exposed*
A, nunbor of irregular Quart* lonooe nlso occur, apparently near
tho trnnovor&o faulte, but tho oro doe o not AB c. rule occur
In tho 'qu'nrts itsolf*
Pyrrhotito cnpoara prftc*ioally nbocnt f row thle vein fctt
*
surfnoo, bat It will jaoat probably cono in Bt gro&tor depth
In tht* chief dove-loped copper property in tho dlotrict,
pyrrhotite nr\do ito firot appeixranoo at the COO-ft. lcvol,
trhoro it occurs in wr.ocivo ctrincoro. ^!he r.inernl l e not
of vr.luo in Itsolf, but Ito tendency towardo o noy replace—
r.ont by cluxlcopyrito lo voll-ootftT)liohod*
0?H "I
Two cuarts Tolno hcxvo been found e&tJt of thle smin vein,
Aloo o vnin of pure c&loito, but values of oonooqucnoo hnvo
not os yot boon found in thooo voino* '
Oron of r.iodiuci to hl^h crado brought out in the courao
of davnlopnioui o^-uld bo ohippad to the X o r and a emolter, on
r.o-onnt of tho oxoeptlonnlly favourable oltuatlon of tho
pro;j'.?rty v.-iti; regard to transportation* There le very
litilo of n rofrnotury nataro In tho oro, nhich should be
fit 'ho ordlnr^ry l^aoo rato of Ktout C-^*00 por ton*
- 10 -
l?A7u:r: Ajn nini'o,:;^;. up GJP-:^It lo bollovel that tho "breaking point" for profitable
shipments would bo about flvo ?or cent copper* A carload
of oro runv.lnfT between flro and ton por cent could probably
bo assembled alnou t Ir.noilatoly frora tho dunps of ; tho ttro
veins* Thorn la a vorj reasonable hope thai cufiloiont
ore sill bo dovolopoJ In thlo dlatrlctto juotlfy tho ©root-
ion of a flotation qonocntrator*
tt -'O or . :^:iii T r ONn i
l* Thn incline shaft should be continued to Ito pronont ol'jootivo of 50 foot*
2. ^ho vein area to tho north find south of tho nen dts-* oovoryx ahoiild bo thoroughly otripped t/SvcroTfor dopth of overburden and water conditiono porralt*
S* Tho vein Itoelf chould bo bladt trenched nt Intervale of oay 50 mot and toct pita ohould bo put dovfn at f?,riov,3 polnto to dotcrraino any chan;;oe in character of nineraliaation*
4* tho plokot lino striklnr? north 20 flogreos nctlc) should bo oxtondoJ both north nnd couth to f\ituro tronchlnc nr.d drilling operation©*
weettxs a guido
5. Tondoro ohould bo c&lled for t^o thouocnd foet of dlancnd driljlr./r- Thi0 foota^o cou.ld bo usefully omployod in drill in,; a nerioo of SOO-ft holca to tost both structure r-, r. A vein ut vortical depths of rk pproxtnately 200 foet. To do t.'. ir it v.'oulil *oo nccococry to drill fr^ri tho enst ir. to*ardo tho dip of tho voin, ;;i7inr; tho hoi 03 nnd initial dip of tilout 55 dogmas voat* Uitoo for ouch drill holes to bo ocl^otod on tho results of tho curfp.co work novr being
out.
6. A nnf-notonotT c urvoy would proo&bly proro ofIn trr.tiin- o;;t th* nnrth.-rr. oxtor.olon of tho voin {cnotvoln) In thr lov, ovrrburdonod ,-ruur.d3.000 font rort.'i of Iht* ii.oli;^ rJ-.rvft.a vory Intrr^ntin^ nron* ;. fow northtV.** pick-C'tO'I VMIC )ino eho.ild Vo ni;f flono t -kon ri t protablli li os r.'or^ r-'-*'*rV"
l a hru^
rr.Mch begins rTM o le potontlnlly
rnd south linoo i\oar obnervat-
Thointervale of 100 foet olon; theoo linoo* r.ro that the otriice of tho v ein w i 3 1 turn tTr.rd tho north, in Conformity with tho u/.i of tho country* -
ft
- n -
H *3or.y?3m tri ON s i
7* Cnro should be taken that nocousftry that p -i r t of tho property hold no raining performe-i and recorded*
assessment work. on alaina la duly
4'ifIr l-1
IL
8* Should tho a'lowinca In tho neighbourhood of the non dis- oov**ry otand up to thoir pronnnt pronlna in the coiireo of further work, tho sinking of another exploratory incline Bhtvft in thio r. roo. w j aid bo
Aosayo wore nad o by tho Provincial Assayere Office, ?arliat3ont Buililin^s, toronto, froa vhon pulps for checking purpoo os can to ob tained nt Any titio within cix months*
9RIOHT* BOYI*v:Ll. f JAIISS ft ASSOCIATES Consul ting i-ir.iiij;
Par
VOHOJITO, July 12, 1929*
COMPANY ^.Wajrr en.. ExplQ.j:a,t.jLana..Limited-...
PROPERTY ......Gawley...Opt.....Catharine...THp-...-...
DIAMOND DRILL RECORD HOLE NO. ...Hinki. J.,
SHEET NO. l DATE Dec. 23, 1974
DIP ANGLES
0' - 450
FOOTAGE
0-9'
9' - 36.5'
36.5 - 38
38 - 45
45 - 46.5
46.5 - 78
78'
^
^P
NAME OF ROCK
Casing
Dacite
Andesite -Gabbro
Gabbro
Andesite -Gabbro
Andesite
BEARING 2680 Astronomical ;LENGTH 78 '
LOCATION Grid Line 4 N 80' E
LATITUDE 200' south of northDEPARTURE Boundary
ELEVATION 5,1/2 Lot II Con IV
ROCK Basic to intermediate volcanic rocks.DESCRIPTION
Overburden (Casing left in hole).
Quite siliceous pale gray green fine grainedoccasional calcite stringers up to 1/4 inch inthickness at 45O to core axis. Minor and veryOccasional pyrite.
Contact zone possibly flow contact breccia or intrusivcontact. Slightly darker than above
Dark rather crystalline fine to medium grained black.Minor calcite stringers at 45O to core axis. Someslight fragmentation on contacts of zone. Minorchalcopyrite blebs but less than 5 7, sulphides
Similar to 36.5 - 38
Pale green, occasional calcite stringers at 45O to
core. Volcanic flows. .r
End of Hole.
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Nov. 25, 1974Dec. 10, 1974
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COMPANY Warren Expdorations Limited
" PROPERTY Gawley Opt ^ Catharine Twp.
DIAMOND DRILL RECORD
SHEET NO. l
HOLE NO. .
DATE Jan, 3, 1975
DIP ANGLES
0' - 500
BEARING 2680 AstronomicalLENGTH 5g 1
LOCATION Grid 325' N 90' E
UTITUDE 275' South ofDEPARTURE North Boundary
ELEVATION s| Lot II Con. IVROCK Basic to Intermediate Volcanic Rocks
FOOTAGE
0' - 5'
5' -, 29'
29'
29' - 34'
34' - 56'
56'
A™
A
NAME OF ROCK
Casing
Andesite
(Breccia)
Gabbro
Andesite
DESCRIPTION
Overburden Casing pulled out,
Pale green fine grained*6alcite ^stfeingers at V450to core axis no mineralization (greenstone)
Contact Zone
Flow or intrusive, calcite stringers^medium grainedto fine. Some scattered blebs of Cholcopyrite
As above.
End of hole Core stored in Haileybury at Pione
Reason for Drilling W-2To test depth possibilities of chalcopyritemineralization in trench.
RESULT OF DRILLING W-2
Results inconclusive as light equipment froze up incold weather. Hole not completed.
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^'v 1mCOMPANYPROPERTY Ga*Lle? Opt^Catharine Twp.
DIAMOND DRILL RECORD
SHEET NO. 2
HOlE NO.DATE Dec. 23, 1974
DIP ANGLES BEARING LATITUDE
LENGTH DEPARTURE
LOCATION ELEVATION
ROCK
FOOTAGE
*
0
NAME OF ROCK DESCRIPTION
-Reason for Drilling Hole 47*0.Pile of hirarade ore (approx, 75 tons) of copper-^silver ore beside pit which assayed 8Z Cu. and 1 oz ofAg per ton led us to believe that there could be aplumb of ore large enough to mine and ship to acustom mill. Note Grab Samples only.
Result of Drilling Hole W-lW-l undercut the pit at approx. 20' and encounteredonly minor chalcopyrite mineralization.
Conclusion:More detailed drilling would hayje to be done alongstructure to eliminate possibilities of lenses ofore.
^
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iitnmaFIELD OFFICE
P.O. BOX 39, HAILEYBURY. ONT. PHONE 703-672-3311
To the Shareholders, Warren Explorations Ltd.
Your directors are pleased to submit herewith the initial report on the company's progress since incorporation.
Based on the successful completion of a financing program designed to provide $150,000 in working capital through the placement of 500,000 shares at 30(fc, a preliminary v/ork program was carried out on a 24-claim holding in Catherine and Pacaud Twps., southeast of Kirkland Lake in Northern Ontario.
These claims covered a high-grade surface showing of copper mineralization with supplementary silver values. Your company's program involved geophysical work, limited drilling, and supporting surface work. Two shallow holes were completed, following which work was suspended for the winter months. Drilling will be resumed later to check out some geophysical features.
More recently, and in reflection of the high interest generated by drill-hole confirmation of a new uranium potential in the Sandfly Lake district northwest of Lac LaRonge in Saskatchewan, your company has acquired a 60-claim property to the south of the Thor Explorations discovery group, on which Noranda Mines and Brascan De velopment are financing and conducting an extensive ex ploration program .
The Warren ground lies on strike of the discovery zone, and within the favourable meta-sedimentary belt, The discovery group attracted attention when an extensive assembly of boulders in which encouraging uranium values were obtained were located over an area some 5,000 ft. in length and 300 ft. in width. The Noranda-Brascan team, in their initial diamond drilling, reported an intersection of 3.52 Ibs. U308 over a core length of 13.3 ft.
A field program for the VJarren ground is now being considered, and shareholders will be advised of developments,
...7
smoRATtoHs LIMIT f DFIELD OFFICE
P.O. BOX 39, HA1LEYBURY. ONT.
PHONE 705-673-3311
SUITE 40136O BAY ST.. TORONTO. ONT.
PHONE 416-363-7381
- 2 -
At the same time, your company is pursuing active con sideration of an overseas gold exploration project, but at this point negotiations have not advanced to the point where the potential commitment could be considered as finalized.
On beha3rl\ of the Board of Directors,
Q.hn Pollock, President.
January 18, 1975-
31M13NW8897 63.3246 PACAUD 050
REPORT
ON
THE CATHERINE-PACAUD TOWNSHIPS PROPERTY
OF
WARREN EXPLORATIONS LIMITED
BOSTON CREEK AREA
DISTRICT OF TEMISKAMING
ONTARIO
by L. J. Cunninghon, B.Sc., P.Eng.,Mining Engineasr
dated at Kirkland Hake, Ontario3rd July, 1974
TABLE OF CONTENTS
, Page
SUGARY
INTRODUCTION l
LOCATION fc ACCESSIBILITY 2
GENERAL GEOLOGY . 2
GEOLOGY OF THE PROPERTY 2
ECONOMIC GEOLOGY OF THE AREA 3
ECONOMIC GEOLOGY OF THE PROPERTY 3
CONCLUSIONS ft RECOMMENDATIONS 4
CERTIFICATE
MAPS:
1. Location Map - Kirkland-Larder Area
2. Claim Map - Part of Catherine fe Pacaud Tovmships
3. Map 1957-4 - Geology of Boston Township and
part of Pacaud
In pocketof
report
SUMMARY OF A
REPORTON
THE CATHTJilNE-PACAUD TOWNSHIPS PROPERTYOF
WARREN EXPLORATIONS LIMITEDBOSTON CREEK AREA
DISTRICT OF TEMISKAMING .ONTARIO
1. The property consists of two contiguous patented lots, one in Catherine
Township, the other in Pacaud Township of the Larder Lake Mining Division,
Ontario,
2. Small b\it rich pipe-like copper deposits are found associated with volcanic
rocks in a zone extending for at least three miles along the eastern margin of
the Round lake batholith.
3. Shaft sinking and mining has been done on 4 of these deposits and a limited
tonnage of high grade copper has been shipped as direct smelting ore.
4. The Warren ground includes the former Mindoka property on which a 115 foot
shaft was sank and from which 225 tons of 8ft copper were shipped to the Noranda
smelter.
5. The property has been idle since 1929.
6. A program of line cutting, magnetometer and EM surveys, and a 2,000 foot
drilling program are recommended to test for zones of massive copper-bearing
sulphides.
Estimated cost of the program is $33,000.00.
3rd July, 1974
KEPORTON
THE CAT11ERINE-PACAUD TOWNSHIPS PROPERTYOF
WARREN EXPLORATIONS LIMITEDBOSTON CREEK AREA
DISTRICT OF TEMISKAMINGONTARIO
INTRODUCTION'In the early 1920's the Boston Creek Area was actively prospected for
gold and a limited production was obtained from two properties.
In 1926 copper vras discovered' along a zone extending southeasterly for
2-J, miles from the Village of Boston Creek. Between 192? and 1930 a limited
production was obtained by underground development of three properties.
Similar rocks extend in a semicircular belt along the periphery of the
granite through Catherine Township and contain a number of known gold and copper
showings.
During 1974 Jonpol Explorations Limited purchased the property for
^6,000.00 cash and a yfa royalty based on net smelter returns to a maximum of one
million dollars, thereafter the royalty will be reduced to 2# of net smelter
returns. Jonpol Explorations Limited are vending the property to Warren
Explorations for a stock consideration.
The property covers the favourable copper bearing horizon and is
considered a base metal prospect.
The following references have been utilized:
Grant, James A. Geologist, Ontario Department of Mines Geological Report No,18 Catherine fe Mater Townships
Lawton, K.D., Geologist, Ontario Dept. of Mines "Geology of Boston Townshipand Part of Pacaud Township" Vol. 66 pt. 5, 1957 with map 1957-4
Koiles, R.G. Ph.D., Geological Report on the Trethewey-Ossian Lease of the GoldenArrow Mines Ltd., Pacaud Township, Boston Creek Area, Ontario dated June 15th, 1952
Ennis, G.F., Mining Engineer, Report on Ossian-Trethewey Copper Property, PacaudTownship, Ontario dated January 25th, I960
Bell, R.A., Geologist, Report on the Induced Polarization and Resistivity Resultsfrom the Boston Creek Property, Pacaud Township, Onta rio for Fidelity Mining Investments Limited dated ?th December, 1961
Cunningham, L. J. Mining Engineer, Report on Patterson fc Trethewey-Ossian CopperProperties, October, 1966
James, Victor A., Mining Engineer, Report on Mindoka Mines Limited, July 1929
Hughes, Frank W., B.Se., Mining Engineer, Report on Copper in Pacaud Township,November, 1953
/arren Exploration, Horton Creek
LOCATION 6 ACCESSIBILITY
i 2 July 1974
Tlie property consists of 2 contiguous patented lots, one in Pacaud
Township, the other in Catherine Township.
They are unnumbered but are described as follows: -ri Pacaud Township Sg Lot l Con. IV 160 acres
Catherine Township S| Lot 12 Con. IV 152 acres
The property lies approximately 14 miles southeast of the Town of
Kirkland Lake. The claims are 8 miles east of Highway 112, Highway 564, an all-
weather gravel road., extends easterly from Highway 112 through the village of
Boston Creek and then turns southerly to cross the centre of the property along
the Pacaud-Catherine Townships line.
A high tension power line of the Ontario Hydro Electric Commission,
and the Ontario Northland Railway are located about 3/4 of a mile southwest of the
property. The railroad is accessible by an all-weather gravel road, the distance
from the property being three miles.
GEHKPJVL GEOLOGY
Keev.-atin volcanic rocks underlie most of the areaj immediately to the
west is the Hound Lake granitic pluton, with its margin convex to the east. In
eneral conformity vtith this margin are: (a) banded tuff, (b) basic to inter
mediate lavas and intrusions, (c) intermediate to acid fragmental rocks, and (d)
coarse-grained volcanic rocks.
The Keewatin rocks were intruded first by ultrabasic to intermediate
dikes and sills, and then by numerous, small acid to intermediate, and lampro
phyric dikes - probably associated with the emplacement of the Round Lake pluton.
JEOLOGY OF THE PROPERTY
The eastern margin of the Round Lake pluton underlies parts of Lot 12
along the western edge of the property. The Keewatin rocks occur as a steep
anticlinal belt around the granite. Grant (O.D.M, G.R. 18) has subdivided these
rocks into three stratigraphic formations, from west to east and from oldest to
youngest as follows:
A. Interbedded tuff and tuffaceous sedimentary rocksj with minor iron formation.
This division lies next to the Round Lake pluton and is traversed by numerous
small dikes and sills. The total thickness is unknown, but is about 1,300 feet
here,
B. Dioritic, dacitic, and andesitic lavas. Pillowed lavas are common in this
division, which has a thickness of about 10,000 feet.
I'/urren Kxplcration, Boeton Creek
C. Porphyritic and aphanitic, intermediate to acid volcanic rocks, largely
pyroclastic, and agglomerate. The thickness of this division is also about
10,000 feet.
Thus the following sequence of rocks exists across the property from
;est to east:
1) a north south strip of granite ~ 1/2 mile wide being the edge of the pluton
2) a belt of interbedded tuff and tuffaceous sediments, 1/4 mile wide, striking
jortherly with steep easterly dips
3) a band, 2 miles wide, of basic lavas with similar strike and dips 0
A basic sill some 500 feet in v;idth parallels the granite contact
jithin the basic volcanics and forms the east boundary of the property. It is a
dark grey, medium grained quartz gabbro.
Minor amounts of Keweenawan diabase and Algoman syenite, quartz
porphyry arid lamprophyre occur as small irregular intrusions or dikes*
A number of faults extend radially to the east from the granite
Dluton into the Warren ground. :
SCONCMIC CPJOLOGY OF THE AREA
- 3 ~ July, 1972,
Two miles to the northwest of the Warren ground copper shoots have beei
nined as replacement bodies in iron formation at the contact with acid tuff.
The mineralized zones are pipe-like and of high grade (5 to 10^ copper
per ton) with maximum dimensions of 50 feet in length by 5 feet in width. They
appear to be localized at cross faults which cut the iron formation.
The ore consists of chalcopyrite v/ith varying amounts of bornite,
chalcocite, pyrite and pyrrhotite. Mineralization grades rapidly from massive
halcopyrite to barren pyrite and pyrrhotite.
Three adjoining properties, the Amity, the Patterson and the Trethewey-
Ossian, were explored by underground development. Some stoping was done and limit'
tonnages of direct anelting copper ores were shipped to Noranda during the 1920's.
Since that time, these three properties have been leased and a small
amount of high grade (5# ~ 10#) copper has been salvaged. Limited drilling has
been done on some of these properties.
ECONOMIC GEOLOGY OF THE PROPERTY l , ,
Within 200 feet of the Pacaud-Catherine Township line in the northwest
quarter of Lot 12, Con. IV Catherin Township, the caved collar of a small shaft
can be seen v/ith a small rock dump. Caved and flooded trenches indicate the
presence of two veins which are described by Victor A. James, Mining Engineer, in
arren Explorations, Boston Creek~ 4 -
July, 1974
, report dated 12th July, 1929 as follows:
"The westerly vein system occurs practically on the Pacaud-Catherine
ownship line, very close to the granite contact. The contact itself lies in low
round, but has been established by diamond drilling. Granitic dykes (or small
sills) also occur along the bedding planes of the tuffs near the veins.
The veins consist of stringers of fairly massive chalcopyrite, together
;ith about two feet of banded pyrite and chalcopyrite mineralization in silicified
uffs e The veins follow the bedding of the tuffs and dip about S2 degrees east.
Two of the nain stringers are 45 feet apart. A vertical 2~corapartment shaft 100
feet deep was sunk on the easterly one, and 55 feet of crosscutting was done at
he 100-ft. level. These workings are now under water and the information below,
obtained from the superintendent in charge, is given as a matter of record.
Two drift rounds on the vein from the west crosscut showed 4# copper
over a width of 4 feet and 5# copper over 4 feet.
Four diamond drill holes were also put down. Three of these disclosed onditions ranging from mineralization to ore. The best hole showed 21 inches of
ore, representing 10y plus inches true width, of massive chalcopyrite assaying
2I?3 copper. A ?0-degree hole cut 6 feet of vein matter assaying 2.6# copper.
In general,,it may be said that this depth exploration slightly
bettered the condition appearing on surface, but the dimensions established to
date are rather too small to constitute an economic deposit,"
Frank W. Hughes, B.Se., Mining Engineer, in a report on the copper
properti.es of the Boston Creek Area dated l?th November, 1955, described the
lindoka property as follows:
"Mindoka Mines; Shaft 115 ft.- one level established. 3 D.D. holes
from surface. D.D, Hole #1 intersected 18" true vddth massive chalcopyrite at
vertical depth of 250 ft. D.D. holes #243, along strike for an overall lengthi
of 400 ft. intersected 2" to 3" stringers of chalcopyrite over 6 to 7 ft. at
vertical depth of 250 ft. Previous operators shipped to Noranda in 1929: 225 tons
of S?3 copper."
INCLUSIONS St RECOMMENDATIONS
The property has been idle since 1929. Consequently caving, flooding
and the overgrowth of brush and trees has obliterated almost all evidence of the
two known veins. However there is no doubt that Mr. James and Mr* Hughes are
describing the occurrences on the Warren ground.
Work to date on the Boston Creek copper belt has produced small, rich
'/arren Explorations, Boston Creek - 5July, 197/1.
pipe-like bodies of copper mineralization. However, this does not preclude the
possibilities of finding zones of rich mineralization of a size to permit economic
xtracvtion. The geology is favourable and the physical features, such as good
road access, close proximity to rail shipping facilities and smelter, operations
(Koranda, Quebec) are distinct advantages in the successful mining of small or
large ore bodies.
In 1970 an airborne Questor Mark MKV input survey was flown over the
area by Moncrieff Uranium Mines Limited. Mo conductors were reported on the Warrer
ground but a re-exanination of the flight tapes is recommended. The Warren ground
was not held by Moncrieff, consequently little attention may have been given to
this portion of the survey.
It is further recommended that:
(i) Lines be cut at 200 foot centres across the Catherine half of the property
(ii) Lines be cut at 400 ft. centres across the Pacaud half of the property
(iii) A magnetometer Si a VLF survey be completed over the property
The Catherine half of the property be mapped(iv)
(v)
Estimated Cost
$ 1,300.00
700.00
2,500.00
1,000.00
Diamond drilling be completed to test:(a) anomalous areas(b) the known veins at shallow horizon and in the
vicinity of the shaft
2,500 feet @ 10.00/ft.
Supe J'vision
25,000.00
2,500.00
$ 33,000.00
Signed,
Dated atKirkland Lake, Ontario3rd July, 1974
L. J. Curininghara, B.Sc,, P.Eng., Mining Engineer- . '-
V W
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Warren Explorations Ltd.
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A
PROVINCE
OF ONTARIO
PROVINCE
OF QUEBEC
ONTARIO
DEPARTMENT O F MINES
HON. (i. O.WAKDKOPK, M inister of Mint*
IX P. Douglas1*. Deputy Ministcr M . K. Hurst, D irector, Geahffica! llranch
Map 2043Catharine a nd Marter Townships
WAEEEN
LIMITED
T a*^f ; iCsr ^
SYMBOLS Scale, l inch to 50 miles
N.T.S. reference 31 M/13,32 D/4,: ^ ! ^: iGlacial striae,
Small rock outcrop.
Boundary oj rock outcrop.
Geological boundary, defined.
Geological boundary, approximate.
Geological boundary, assumed.
^' ;^m r
H, f A .,
anrf tf/p o f schistosity,
Strike of vertical schistosity.
Strike and dip of gneissosity.
Strike of vertical gneissosity.
Jointing, inclined.
;1M v*} ^
PLEISTOCENEClay, sand and gravel.
PRECAMBRIAN**PROTEROZOIC
KEWEENAWAN
\ a '' ' i ^- \ \ feb ,'-' )'",*;' "\ ^ )-\ * '''' -r-, f /l/V^----- \ 3t \ M \ \ \ i \ l f f V-^ . \ 1*^-'( i, o N i 26; r /~'
,—— ' V-' l\* '"^ -""' 7 ^'
HURONIAN COBALT GROUP
GOWGANDA FORMATION5a Conglomerate. 5b Greywacke. 5c Arkose, quartzite. 5d Argiiiite.
ARCHEANALGOMAN?
4a Syenite.4b Granodiorite,4c Granodiorite gneiss (Round Lake
pluton). 4d Albite porphyry, quartz-slbite
porphyry. 4e lamprophyre. 4! Felsite.
3a Diorite.3b Gabbro.3c Serpentinized peridotite.3d Diorite porphyry, dacite porphyry.
KEEWATINBASIC TO INTERMEDIATE
VOLCANIC ROCKS(prodom;nantly lavas)2b Dacite and andesite, including
2 pillow lavas.2c Diabase, diorite and gabbro. 2f Sheared volcanic rocks. 2g Fragments/ iavas. 2v Variolitic lavas.
INTERMEDIATE TO ACID VOLCANIC ROCKS
(predominaitly pyrcclastic)1a Porphyritic dacite and andesite,
mostly crystal tuff.Jb Dacite and andesite, mostly
aphanitic tuff.1d Banded luff and tuffaceous sedimen
tary rocks with minor iron formation1f Sheared volcanic rocks.1g Agglomerate.1r Rhyolite.
CATHARINE
LOCATION PLAN OF MINING PROPERTIESScale, l incti to 2 miles
?. Burnand-Gzowski.2. Cam p bel!.3. Canoro (Q&tmm).4. Catharine Gold.5. Connett-McDonougn.6. Cotter.7. Daley.8. Gold Hi!!. 3. Hounsiow.
W. Katyniuk.11. Kennedy-Boston.12. Kordo! Explorations Ltd. (Gold Bank).13. Kordo! Exolorations Ltd. (Gold Ridge).14. Minaoka.15. Mirado Nickel Mines Ltd. (Caihroy Larder). W. Ostrom.17. Roger-Barnett.18. Sawka Aiisrd.W. Tyrzonc Explorations Ltd. (Hilltop).20. Walsh-T ay lor.21. Wojcieszyn,
Map 2043
CATHARINE AND MARTER TOWNSHIPSTIMISKAMING DISTRICT
20©
Sralt- 1:31,680 or l Inch tn '/j Milr
Feet 1000 &.000 10,000 Feet
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RADEM SURVEY CONDUCTORS - —————— —
STATION USED - CUTLER, MAINE
WARREN EXPLORATIONS LTD.:
3IM13NW0C97 63.3246 PACAUD 320
RADEM SURVEY
PACAUD 8. CATHERINE TWPS
SCALE I'VIOO' JAN. 1975
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